The Removal of Dissolved Metals by Hydroxysulphate Precipitates during Oxidation and Neutralization of Acid Mine Waters, Iberian Pyrite Belt

Author:

España J. Sánchez,Pamo E. López,Pastor E. Santofimia,Andrés J. Reyes,Rubí J. A. Martín

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference43 articles.

1. Basaluminite and Alunite: A Possible Cause of Sulfate Retention by Acid Soils1

2. Alpers C.N. and Nordstrom D.K. (1999) Geochemical modeling of water-rock interactions in mining environments. In The Environmental Geochemistry of Mineral Deposits, Part A. Processes, Techniques, and Health Issues (eds. G.S. Plumlee and M.J. Logsdon), Society of Economic Geologists. Rev. Econ. Geol. 6A, 289–323.

3. Ball, J.W. and Nordstrom D.K., 1991. User’s manual for WATEQ4F with revised thermodynamic data base and test cases for calculating speciation of major, trace, and redox elements in natural waters. pp. 91–183, 189. U.S. Geological Survey Open-File Report.

4. Effect of Ca2+, Mg2+, and Anion Type on the Aging of Iron(III) Hydroxide Precipitates

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